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首页> 外文期刊>ournal of the Meteorological Society of Japan >Lidar Measurements of Stratospheric and Tropospheric Aerosols at 1064 nm Using a New and Low-Noise Photomultiplier
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Lidar Measurements of Stratospheric and Tropospheric Aerosols at 1064 nm Using a New and Low-Noise Photomultiplier

机译:使用新型低噪声光电倍增管在1064 nm处平流层和对流层气溶胶的激光雷达测量

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Using a new type of photomultiplier (PMT) tube R3236 cooled to -30°C, and a photon counting method, lidar measurements of stratospheric aerosols and tropospheric aerosols above an altitude of 2.25 km were made at the fundamental wavelength ofλ=1064 nm of a Nd:YAG laser which is sensitive to aerosol scattering. The PMT R3236 was found to be useful even for measurements of stratospheric aerosols near the background level.The average of the integrated backscattering coefficient above tropopause was 3.3×10-5 sr-1 at Tsukuba (36.1°N, 140.1°E) during November through December 1988. Tropospheric aerosol layers in the free atmosphere were frequently observed and the altitude of the maximum scattering ratio of the aerosol layer varied for every measurement, compared with the stable stratospheric aerosol layer. Some tropospheric aerosol layers were confined by two inversion layers.
机译:使用冷却至-30°C的新型光电倍增管(PMT)R3236和光子计数方法,在λ= 1064 nm的基波波长下对海拔2.25 km以上的平流层气溶胶和对流层气溶胶进行激光雷达测量。 Nd:YAG激光对气溶胶散射敏感。发现PMT R3236甚至对测量背景水平附近的平流层气溶胶也很有用.11月,筑波(36.1°N,140.1°E)在对流层顶上方的平均反向散射系数平均值为3.3×10-5 sr-1。直到1988年12月。在稳定大气中经常观察到对流层气溶胶层,与稳定的平流层气溶胶层相比,每次测量的气溶胶层最大散射比的高度都不同。一些对流层气溶胶层被两个反演层所限制。

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